Table Of ContentLP1 Contribution No. 790 47
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SEARCH FOR A METEORITIC COMPONENT AT THE relative to the sandstone, the invoked additional component is
BEAVERHEAD IMPACT STRUCTURE, MONTANA. Pas- unlikely to be chondritic or iron-rich meteoritic material. Instead,
cal Lee1 and Robert W. Kay2, 'Department of Astronomy, Cornell the low Ni/Cr ratio in the breccia and the melts points either to an
University, Ithaca NY 14853, USA, 'Department of Geological achondritic impactor or to some other (terrestrial) source of Cr
Sciences. Cornell University, Ithaca NY 14853, USA. enrichment.
Meteoritic geochem ic al signatures at large and/or ancient terres-
The Beaverhead impact structure, in southwestern Montana trial impact craters are difficult to find [3]. Possible reasons for this
(44°36-N;112°58'W), was identified recently by the presence of include the high impact velocities and energies involved in large
shatter cones and impactitcs in outcrops of Proterozoic sandstones impacts, the possibility of chemically inconspicuous (achondritic)
of the Belt Supergroup [1]. The cones occur over an area > 100 km1. projectiles, weathering and hydrothermal alteration of impactites
Because the geologic and tectonic history of this region is long and and their associated country rock, and inadequate sampling. Our
complex, the outline of the original impact crater is no longer search for a meteoritic component in samples from the Beaverhead
identifiable. The extent of the area over which shatter cones occur impact structure will be discussed in the context of this general
suggests, however, that the feature may have been at least 60 km in problem.
diameter. The absence of shatter cones in younger sedimentary units References: [1] Margraves R. B. ct al. (1990) Geology. IS.
suggests that the impact event occurred in late Precambrian or early 832-834. [2] Koeberl C. and Fiske P. S. (1991) Meteoritics, 26.
Paleozoic time. 358-359. [3] Palme H. el al. (1978) CCA, 42, 313-323.
We have collected samples of shocked sandstone from the so-
called "Main Site" of dark-matrix breccias, and of impact breccias
and melts from the south end of Island Butte. The melts, occurring
often as veins through brecciated sandstone, exhibit a distinctive ORDOVICIAN IMPACTS AT SEA IN BALTOSCANDIA. M.
fluidal texture, a greenish color, and a cryptocrysUuline matrix, with Lindstrom1, V. Puura2. T. Floden1. and A. Bruun3, 'University of
small inclusions of deformed sandstone. Samples of the same type, Stockholm, Sweden, 'Estonian Academy of Sciences, Estonia,
along with country rock, were analyzed previously for major- and 'Swedish Geological Survey. Sweden.
trace-element abundances [2]. It was found that, although the major-
element composition was relatively uniform, the trace-element Northern Europe has an assemblage of Ordovician probable
composition showed variations between the melt material and the impacts that is exceptional because the structures involved are
adjacent sandstone. These variations were attributed to extensive relatively old yet well preserved because they formed at sea and
weathering and hydrothermal alteration. because they formed within a restricted geological time in a
In a more specific search for a possible meteoritic signature in relatively small area. The Tvaren. Kardla, and Lockne structures
the breccia and the melt material we have conducted a new series of might not be strictly contemporaneous but all formed near the
trace-element analyses on powders of our own samples by thermal beginning of the Caradoc Age (about 460 Ma), whereas die Granby
neutron activation analysis. Our results indicate that IT abundances structure is about 20 Ma older. The range of diameters is from about
in the breccia, the melts, and the adjacent sandstone clasts are no 2 km (Tvaren, Granby) to 8 km (Lockne). The s tratigraph ic succes-
greater than about 0.1 ppb, suggesting no IT enrichment of the sion formed on impact at sea, as uniformly documented by these
breccia or the melts relative to the country rock. However, both the structures, begins with a breccia lens consisting of basement rocks
breccia and the melt material exhibit notable enrichments in Cr (8- that are intensely crushed. Owing to expulsion of sea water by the
and 10-fold), in U (9- and 5-fold), and in the heavy REEs (1.5 and impact, this breccia formed under essentially dry conditions. Later
3-fold), respectively (normalization carried out relative to La) (see on this breccia was in part hydrothermally altered. It is overlain by
Table 1). Such enhancements relative to die country sandstone backs urge turbidite that formed from fragments of local sedimen-
suggest that weathering and hydrothermal alteration alone might tary bedrock and crystalline basement when the sea water returned
not be sufficient to account for the observed variations in trace- to the crater site. Either die turbidite is simply a Bouma sequence
element abundances, and that the incorporation of a Cr. U, and (although quite thick—as much as over 50 m) from very coarse
HREE-rich component in the breccia and the melts is likely. rubble to mud, or it is more complex.
Because both the breccia and the melts show no Ir or Ni enrichments After deposition of the backsurge turbidite, or turbidite complex,
the craters still remained as 150-200-m-deep holes in the sea bed.
Together with the presence of relatively shallow water over the run
wall, this situation created predictable hydrologic conditions for
TABLE 1. Trace-element concentmiom in ppra extended histories of sedimentation and biological development at
("1" indicates 2-sigma measurement error). the crater as well as within it For instance, hypoxia frequently
developed in the bottom water before depth had been appreciably
BUSS BUM BHB
reduced by sedimentation. The insights acquired at these craters
Cr 17.76±0.6 1Z7.88±0.5 71.94±0.4 make it possible to improve paleoecological reconstructions ap-
Ni 14.50±2J 15.65±1.0 7.6810.9 plied to Ordovician sea beds.
U 1.4810.1 5.54±O2 6.9910.3 The presence of a concentration of craters within a limited area
Yb 1.38±0.1 3.23±0.1 1.1310.1 of well-preserved and accessible Ordovician deposits raises a
Ta 0.39±0.1 1.6610.1 1.3310.1
question about the Ordovician, especially its middle portion, as
La 5Z49±O5 39.04±0.3 26.4910.2
potentially an age of relatively intense impact activity even in wider
Ir <0.1 ppb <0.1 ppb <0.1 ppb
areas. In this connection it may be apposite to mention that the only
BHSS = Beaverhead undftooe (country rock). BHM = Beaverhead impact fossil stony meteorites so far recorded in rocks are from the late
melt BHB = Beaveihead dark-matrix breccia. Early and the Middle Ordovician.
